We provide correlated observations of enhanced dayside whistler-mode waves and energetic electron acceleration collected by the CLUSTER and GOES satellites during the 23～24 September 2001 storm. Energetic （〉0.6 MeV...We provide correlated observations of enhanced dayside whistler-mode waves and energetic electron acceleration collected by the CLUSTER and GOES satellites during the 23～24 September 2001 storm. Energetic （〉0.6 MeV） electron fluxes are found to increase significantly during the recovery phase and the main phase, by a factor of～50 higher than the prestorm level. These high electron fluxes occur when strong dayside whistler-mode waves are present. Two-dimensional （2D） numerical simulations are carried out and the results demonstrate that the dayside whistler-mode wave can contribute to such enhancements in electron flux within 24 h, consistent with the observation.展开更多
为了分析台风影响下浙江沿海风和浪的演变特点,利用浙江省海洋浮标站监测数据和欧洲中期天气预报中心第五代全球气候大气再分析数据(European Centre for Medium-Range Weather Forecasts Reanalysis v5,ERA5),选取2010年以来严重影响...为了分析台风影响下浙江沿海风和浪的演变特点,利用浙江省海洋浮标站监测数据和欧洲中期天气预报中心第五代全球气候大气再分析数据(European Centre for Medium-Range Weather Forecasts Reanalysis v5,ERA5),选取2010年以来严重影响浙江的7次台风个例,对台风作用下浙江沿海海面风和浪的演变特点进行分析。结果表明:在台风影响过程中,海浪波型多数呈现混合浪-风浪-混合浪的演变规律;涌浪波型的出现与台风强度及其与浮标站的距离和方位有关,也与海洋潮汐现象紧密相关。台风影响期间,浙江沿海浪高的变化受风速和风向共同作用影响。在风向不变的情况下,持续风速增大对浪高的增大有明显作用;风向的变化也会对浪高变化产生影响,向岸风和离岸风的转变会造成浪高出现剧烈变化。ERA5再分析资料有效波高在台风浪较大时会呈现偏小的趋势,分析订正后的ERA5有效波高发现,台风浪有效波高大值区与台风中心位置相关。研究结果可为严重影响浙江沿海的台风浪预报服务提供参考。展开更多
Almost everything I have done in the last twenty years is based on what I have discovered from studying ocean phenomena.Specifically,the waves on the surface of the ocean and their dynamics.Two items stand out:The fir...Almost everything I have done in the last twenty years is based on what I have discovered from studying ocean phenomena.Specifically,the waves on the surface of the ocean and their dynamics.Two items stand out:The first one is from studying the evolution of the waves from ripples to fully developed giant ocean waves.To quantify the changes,I found that frequency is very different from what had been defined traditionally through Fourier analysis.Ture frequency should be determined by difterentiation of the phase function defined by an adaptive method rather than by any form of integral transform.Therefore,it should have ever changing instantaneous values.The second discovery is from studying wave turbulence interactions.To reveal the detailed dynamics,I found that spectral representation should not be a single line on the frequency and energy plane.True spectrum should be a high dimensional manifold to cover all the possible dynamic interactions:additive and multiplicative ones.These discoveries have enabled me to develop a set of nonlinear and nonstationary data analysis tools to study many other phenomena,from turbulence to brain waves.They have led me to new wonders I have never even contemplated before.展开更多
基金supported by National Natural Science Foundation of China(Nos.40925014,41274165)the Specialized Research Fund for State Key Laboratories,the Aid Program for Science and Technology Innovative Research Team in Higher Educational Institutions of HunanProvincethe Construct Program of the Key Discipline in Hunan Province,China
文摘We provide correlated observations of enhanced dayside whistler-mode waves and energetic electron acceleration collected by the CLUSTER and GOES satellites during the 23～24 September 2001 storm. Energetic （〉0.6 MeV） electron fluxes are found to increase significantly during the recovery phase and the main phase, by a factor of～50 higher than the prestorm level. These high electron fluxes occur when strong dayside whistler-mode waves are present. Two-dimensional （2D） numerical simulations are carried out and the results demonstrate that the dayside whistler-mode wave can contribute to such enhancements in electron flux within 24 h, consistent with the observation.
文摘欧洲环境卫星-高级合成孔径雷达(Environmental Satellite-Advanced Synthetic ApertureRadar,Envisat-ASAR)波模式数据提供了全球风、浪要素信息,在海浪模式预报与同化方面有重要作用。该数据合成孔径雷达(Synthetic Aperture Radar,SAR)图像普遍存在海浪条纹清晰度不同的现象,但是否影响数据精度尚无定论。本文通过比较2010年NODC(the National Oceanographic Date Center)浮标观测数据和波模式数据,发现经过官方修正后的海浪参数反而具有更大误差。进而通过对比不同条纹清晰度的SAR图像反演参数误差,揭示了ASAR产品海浪参数与浮标测量值之间的误差与海浪条纹清晰度的关系。结果表明:海浪条纹清晰的SAR图像的主波波长和主波周期的反演误差更小,而条纹不清晰SAR图像的有效波高和风速的反演误差更小。通过分析海浪参数对海浪条纹清晰度的敏感性,证实了有效波高和方位向截断波长对SAR图像条纹清晰度的响应最好,波陡次之,与卫星飞行方位角和入射角无关。因此,在反演和修正SAR波模式数据时,考虑图像的条纹清晰度,将会有效提高反演数据的精度。该研究可为高分三号等卫星的波模式数据波浪要素反演精度的提升提供有价值的参考。
文摘为了分析台风影响下浙江沿海风和浪的演变特点,利用浙江省海洋浮标站监测数据和欧洲中期天气预报中心第五代全球气候大气再分析数据(European Centre for Medium-Range Weather Forecasts Reanalysis v5,ERA5),选取2010年以来严重影响浙江的7次台风个例,对台风作用下浙江沿海海面风和浪的演变特点进行分析。结果表明:在台风影响过程中,海浪波型多数呈现混合浪-风浪-混合浪的演变规律;涌浪波型的出现与台风强度及其与浮标站的距离和方位有关,也与海洋潮汐现象紧密相关。台风影响期间,浙江沿海浪高的变化受风速和风向共同作用影响。在风向不变的情况下,持续风速增大对浪高的增大有明显作用;风向的变化也会对浪高变化产生影响,向岸风和离岸风的转变会造成浪高出现剧烈变化。ERA5再分析资料有效波高在台风浪较大时会呈现偏小的趋势,分析订正后的ERA5有效波高发现,台风浪有效波高大值区与台风中心位置相关。研究结果可为严重影响浙江沿海的台风浪预报服务提供参考。
文摘Almost everything I have done in the last twenty years is based on what I have discovered from studying ocean phenomena.Specifically,the waves on the surface of the ocean and their dynamics.Two items stand out:The first one is from studying the evolution of the waves from ripples to fully developed giant ocean waves.To quantify the changes,I found that frequency is very different from what had been defined traditionally through Fourier analysis.Ture frequency should be determined by difterentiation of the phase function defined by an adaptive method rather than by any form of integral transform.Therefore,it should have ever changing instantaneous values.The second discovery is from studying wave turbulence interactions.To reveal the detailed dynamics,I found that spectral representation should not be a single line on the frequency and energy plane.True spectrum should be a high dimensional manifold to cover all the possible dynamic interactions:additive and multiplicative ones.These discoveries have enabled me to develop a set of nonlinear and nonstationary data analysis tools to study many other phenomena,from turbulence to brain waves.They have led me to new wonders I have never even contemplated before.
